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Environmental and Social Impact Assessment
Final Environmental and Social Impact Assessment Report for the Proposed 100MW Solar Independent Power Plant and 18 KM Transmission Line Project, Ganjuwa Local Government Area, Bauchi State by Nigerian Solar Capital Partners/Globeleq/ARM- Harith June 2017 100 MW Independent Solar Power Plant, Bauchi State Environmental and Social Impact Assessment Table of Contents List of Tables iii List of Figures iv List of Acronyms and Abbreviations v List of ESIA Preparers viii Executive Summary ix Chapter One: Introduction 1.1 Background 1-1 1.2 Overview 1-2 1.3 Project Scope 1-2 1.4 Project Location 1-3 1.5 Study Objectives and Terms of Reference 1-6 1.6 Report Structure 1-6 Chapter Two: Policy, Legal and Administrative Framework 2.1 Applicable National Policies 2-8 2.2 Applicable National Regulations 2-10 2.3 Institutional Framework 2-14 2.4 Applicable International Agreements and Policies 2-19 2.5 Permit Requirements 2-21 Chapter Three: Project Description 3.1 Project Overview 3-23 3.2 Project Requirements 3-23 3.3 Project Components 3-24 3.4 Operation and Maintenance 3-34 3.5 Project Activities 3-35 3.5.1 Construction 3-35 3.6 Implementation Schedule 3-35 Chapter Four: Description of the Project Environment 4.1 General 4-38 4.2 Study Area and Location 4-38 4.2.1 Reconnaissance Field Visit 4-38 4.2.2 Baseline Data Acquisition 4-38 4.2.3 Sampling Design 4-45 4.2.4 Field Sampling Methods 4-45 4.2.5 Laboratory Methods 4-47 4.3 Bio-Physical Environmental Baseline Condition 4-47 4.3.1 Climate and Meteorology 4-47 4.3.2 Ambient Air Quality 4-52 4.3.2.1 -
The Aim of the Project Is to Carry out Integrated Studies of the Anambra
Preliminary Integrated Hydrocarbon Prospectivity Evaluation of the Bida Basin in North Central Nigeria By N. G. Obaje1, D. O. Balogu1, A. Idris-Nda2, I. A. Goro2, S. I. Ibrahim1, M. K. Musa1, S. H. Dantata2, I. Yusuf1, N. Mamud-Dadi1, I. A. Kolo1+ Abstract The Bida Basin is a NW-SE trending intracratonic structure extending from slightly south of Kontagora in Niger State in the north to the area slightly beyond Lokoja (Kogi State) in the south. All geological maps available on the Bida Basin had lumped the sediments in the basin as one undifferentiated Nupe Sandstone, making it impossible to infer the prospectivity of the basin for hydrocarbon exploration. The delineation of inferred boundaries between the formations in the basin is a significant initial criterion in evaluating the hydrocarbon prospectivity. The formations deposited in the Bida Basin comprise the Bida Sandstone at the base, followed successively upward by the Sakpe, Enagi and Batati Formations in the Northern/Central Bida Basin while the Lokoja, Patti and Agbaja Formations constitute lateral equivalents in the Southern Bida Basin. An institutional research project of the Ibrahim Badamasi Babangida University Lapai (IBBUL), supported by the Niger State Government, has carried out preliminary geological mapping and completed a prospectivity map for the Bida Basin. Geochemical analysis of samples from drilled shallow wells (at Agaie and Kudu) and outcrops was also undertaken along with interpretation of geophysical aeromagnetic data. From the preliminary geological map prepared, prospective areas, ranked as Less Prospective, Prospective and More Prospective are discernable. Geochemical data show that mainly gas and some oil would have been generated within the Prospective and More Prospective sections in the basin. -
Paleoseismology of the North Anatolian Fault at Güzelköy
Paleoseismology of the North Anatolian Fault at Güzelköy (Ganos segment, Turkey): Size and recurrence time of earthquake ruptures west of the Sea of Marmara Mustapha Meghraoui, M. Ersen Aksoy, H Serdar Akyüz, Matthieu Ferry, Aynur Dikbaş, Erhan Altunel To cite this version: Mustapha Meghraoui, M. Ersen Aksoy, H Serdar Akyüz, Matthieu Ferry, Aynur Dikbaş, et al.. Pale- oseismology of the North Anatolian Fault at Güzelköy (Ganos segment, Turkey): Size and recurrence time of earthquake ruptures west of the Sea of Marmara. Geochemistry, Geophysics, Geosystems, AGU and the Geochemical Society, 2012, 10.1029/2011GC003960. hal-01264190 HAL Id: hal-01264190 https://hal.archives-ouvertes.fr/hal-01264190 Submitted on 1 Feb 2016 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Article Volume 13, Number 4 12 April 2012 Q04005, doi:10.1029/2011GC003960 ISSN: 1525-2027 Paleoseismology of the North Anatolian Fault at Güzelköy (Ganos segment, Turkey): Size and recurrence time of earthquake ruptures west of the Sea of Marmara Mustapha Meghraoui Institut de Physique du Globe de Strasbourg (UMR 7516), F-67084 Strasbourg, France ([email protected]) M. Ersen Aksoy Institut de Physique du Globe de Strasbourg (UMR 7516), F-67084 Strasbourg, France Eurasia Institute of Earth Sciences, Istanbul Technical University, 34469 Istanbul, Turkey Now at Instituto Dom Luiz, Universidade de Lisboa, P-1750-129 Lisbon, Portugal H. -
Geology and Geomorphology of the Urema Graben with Emphasis on the Evolution of Lake Urema
Journal of African Earth Sciences 58 (2010) 272–284 Contents lists available at ScienceDirect Journal of African Earth Sciences journal homepage: www.elsevier.com/locate/jafrearsci Geology and geomorphology of the Urema Graben with emphasis on the evolution of Lake Urema Franziska Steinbruch * Scientific Services of Gorongosa National Park, Avenida do Poder Popular 264, Beira, Mozambique article info abstract Article history: The Lake Urema floodplain belongs to the Urema Catchment and is located in the downstream area of the Received 19 December 2008 Pungwe River basin in Central Mozambique. The floodplain is situated in the Urema Graben, which is the Received in revised form 8 February 2010 southern part of the East African Rift System. Little geological information exists about this area. The cir- Accepted 12 March 2010 culated information is not readily available, and is often controversial and incomplete. In this paper the Available online 20 March 2010 state of knowledge about the geology and tectonic evolution of the Lake Urema wetland area and the Urema Catchment is compiled, reviewed and updated. This review is intended to be a starting point Keywords: for approaching practical questions such as: How deep is the Urema Graben? What controls the hydrol- East African Rift System ogy of Lake Urema? Where are the hydrogeological boundaries? Where are the recharge areas of the Lake Floodplain Hydrogeology Urema floodplain? From there information gaps and needs for further research are identified. Lake Urema Ó 2010 Elsevier Ltd. All rights reserved. Mozambique 1. Introduction 2. Regional geology and tectonic evolution The Lake Urema floodplain belongs to the Urema Catchment 2.1. -
Council for Innovative Research Peer Review Research Publishing System Journal of Advances in Physics
ISSN 2347-3487 Evaluation of the Existing State of Geothermal Exploration and Development in Nigeria Sedara, Samuel Omosule1, Joshua,E.O 2 1Oduduwa University, Ipetumodu, Department of Physical Sciences [email protected] 2University of Ibadan, Department of Physics, Ibadan Nigeria ABSTRACT Relatively little expenditure for hydroelectricity and fossil fuels have had a restraining influence on levels of exploration and development for geothermal energy resources in Nigeria for the past several years. The focus of development has been in the areas of low temperature geothermal energy involving the exploration and assessment of hot spring resources primarily for recreational applications – although possibly for other direct uses depending on local infrastructure and access to appropriate energy markets. The geological structure of Nigeria influences geothermal exploration extent within each geological province. Sedimentary basins in Nigeria have been explored for hydrocarbons for several decades, thus the oil companies collected large subsurface temperature data basis. But not much is known about geothermal conditions within Nigerian Precambrian crystalline province. On the basis of BHT data from oil wells it has been found that geothermal gradient in Niger Delta ranges from 1.5 to 4.9°C/100m and in Anambra Basin (directly to the north) it can reach 5.7°C/100m. Exploration for geothermal energy in northern Nigeria based on shallow water wells (down to 600 m deep) was carried out over 20 years ago. The other aspect of geothermal exploration in Nigeria is investigating of the thermal springs and seepages, which occur mainly within sediments of the Middle and Upper Benue Trough. The water of the warmest springs in that area: Akiri and Ruwan Zafi have the temperature about 56°C and it suggests the occurrence of some geothermal anomalies. -
Geophysical Journal International
Geophysical Journal International Geophys. J. Int. (2016) 204, 1565–1578 doi: 10.1093/gji/ggv538 GJI Seismology Ambient noise tomography of the East African Rift in Mozambique Ana Domingues,1,2,∗ Grac¸a Silveira,3,4 Ana M.G. Ferreira,5,6 Sung-Joon Chang,7 Susana Custodio´ 3 and Joao˜ F.B.D. Fonseca1 1Laboratorio´ de Sismologia, 6o, Piso do Complexo Interdisciplinar, Instituto Superior Tecnico,´ Av. Rovisco Pais 1, 1049-001 Lisboa, Portugal. E-mail: [email protected] 2Department of Earth and Planetary Sciences, Birkbeck, University of London, London WC1E 7HX, United Kingdom 3Instituto Dom Luiz, Faculdade de Ciencias,ˆ Universidade de Lisboa, Campo Grande, Ed. C8,Piso3,Gab.5 (8.3.05) 1749-016 Lisbon, Portugal 4Instituto Superior de Engenharia de Lisboa—ISEL, Rua Conselheiro Em´ıdio Navarro, 1, 1959-007 Lisbon, Portugal 5Department of Earth Sciences, University College London, London WC1E 6BT, United Kingdom 6CEris, ICIST, Instituto Superior Tecnico,´ Universidade de Lisboa, Lisbon, Portugal 7Division of Geology and Geophysics, Kangwon National University, Chuncheon, Gangwon-do 24341, South Korea Downloaded from Accepted 2015 December 15. Received 2015 November 8; in original form 2015 May 19 SUMMARY Seismic ambient noise tomography is applied to central and southern Mozambique, located in http://gji.oxfordjournals.org/ the tip of the East African Rift (EAR). The deployment of MOZART seismic network, with a total of 30 broad-band stations continuously recording for 26 months, allowed us to carry out the first tomographic study of the crust under this region, which until now remained largely unexplored at this scale. From cross-correlations extracted from coherent noise we obtained Rayleigh wave group velocity dispersion curves for the period range 5–40 s. -
Biostratigraphy and Palaeoenvironment of Deposition of Nsukka Formation, Anambra Basin, Southeastern Nigeria S.A
Journal of Palaeogeography, 2017, ▪(▪): 1e15 Available online at www.sciencedirect.com ScienceDirect journal homepage: http://www.journals.elsevier.com/journal-of-palaeogeography/ Biopalaeogeography and palaeoecology Biostratigraphy and palaeoenvironment of deposition of Nsukka Formation, Anambra Basin, southeastern Nigeria S.A. Bankole a,*,A.O.Ola-Buraimob a Department of Chemical and Geological Sciences, Al-Hikmah University, Ilorin, Nigeria b Department of Geology, Federal University, Birnin Kebbi, Nigeria Abstract Biostratigraphy investigation of Nsukka Formation was carried out by subjecting well cutting samples obtained from Nzam-1 well to palynological studies with the view towards determining the relative geologic age and palaeoenvironment of deposition of the sediments. Samples were treated in the laboratory through digestion with hydrofluoric acid, sieving with 5 mm, oxidation with Nitric acid and mounting of the slides into sections with DPX mountant. A fairly high abundance and diversity of miospores were recovered, while the interval (847e1372 m) contains distinctive and diagnostic palynomorphs which are stratigraphically important. A Spinizonocolpites baculatus assemblage zone was established based on the basal occurrence of S. baculatus, Spinizonocolpites echinatus, Constructipollenites ineffectus, Periretisyncolpites sp. Peri- retisyncolpites giganteus, Monocolpites sp 1, Foveotriletes margaritae, Syncolporites marginatus, and Longapertites marginatus. The upper part of the interval is marked by association of Anacolosidites -
Paleogene-Early Neogene Palynomorphs from the Eastern Equatorial Atlantic and Southeastern Florida, USA: Biostratigraphy and Paleoenvironmental Implications
Scholars' Mine Doctoral Dissertations Student Theses and Dissertations Spring 2018 Paleogene-Early Neogene palynomorphs from the Eastern Equatorial Atlantic and Southeastern Florida, USA: Biostratigraphy and paleoenvironmental implications Walaa K. Awad Follow this and additional works at: https://scholarsmine.mst.edu/doctoral_dissertations Part of the Geology Commons, and the Geophysics and Seismology Commons Department: Geosciences and Geological and Petroleum Engineering Recommended Citation Awad, Walaa K., "Paleogene-Early Neogene palynomorphs from the Eastern Equatorial Atlantic and Southeastern Florida, USA: Biostratigraphy and paleoenvironmental implications" (2018). Doctoral Dissertations. 2665. https://scholarsmine.mst.edu/doctoral_dissertations/2665 This thesis is brought to you by Scholars' Mine, a service of the Missouri S&T Library and Learning Resources. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected]. i PALEOGENE-EARLY NEOGENE PALYNOMORPHS FROM THE EASTERN EQUATORIAL ATLANTIC AND SOUTHEASTERN FLORIDA, USA: BIOSTRATIGRAPHY AND PALEOENVIRONMENTAL IMPLICATIONS by WALAA KAMALELDEEN AWAD A DISSERTATION Presented to the Faculty of the Graduate School of the MISSOURI UNIVERSITY OF SCIENCE AND TECHNOLOGY In Partial Fulfillment of the Requirements for the Degree DOCTOR OF PHILOSOPHY in GEOLOGY and GEOPHYSICS 2018 Approved by Francisca Oboh-Ikuenobe, Advisor John Hogan David Wronkiewicz Wan Yang Lucy Edwards ii © 2018 Walaa Kamaleldeen Awad All Rights Reserved iii To my daughters, Hala and Sara iv PUBLICATION DISSERTATION OPTION This dissertation consists of the following five articles which have been submitted for publication, or will be submitted for publication as follows: Paper I, pages 3-71 have been accepted by JOURNAL OF AFRICAN EARTH SCIENCES. -
Pull-Apart Basin Tectonic Model Is Structurally Impossible for Kashmir Basin, NW Himalaya” by A
Solid Earth Discuss., doi:10.5194/se-2016-4-AC1, 2016 SED © Author(s) 2016. CC-BY 3.0 License. Interactive comment Interactive comment on “Pull-apart basin tectonic model is structurally impossible for Kashmir basin, NW Himalaya” by A. A. Shah A.nbsp;A. Shah [email protected] Received and published: 10 February 2016 Reply: Dear editor, and the reviewer: Thanks for your time in reviewing my work. I am very pleased to read the comments on my small contribution. The comments are answered below: Comment: Full screen / Esc Anonymous Referee #1 Received and published: 9 February 2016 This paper almost reads like a personal diatribe. Printer-friendly version Reply: Discussion paper I have not written it to attack my colleagues but to discuss science. C1 Comment: SED The author is adamant that the Kashmir Basin is not a pull-apart basin as proposed by Alam et al. (2015, 2016) and the paper is essentially an earnest attempt at refutation. The author calls the pull-apart model ‘impossible’ 15 times (including in the title and Interactive in 110 lines of text) and also states that the pull-apart architecture ‘could not exist’, comment is ‘problematic’ and ‘inconsistent with data’. If one of my undergraduates had written this paper, I would have sent it back with advice to remove the redundancy, improve the English, remove absolute terms like ‘impossible’, eliminate the undercurrents of emotion, and just stick to data-based arguments. This paper is poorly written and should not be published as is. Reply: I am sorry if you felt that I am forcing the reader to believe me. -
Transtensional Folding
Journal of Structural Geology 56 (2013) 89e102 Contents lists available at ScienceDirect Journal of Structural Geology journal homepage: www.elsevier.com/locate/jsg Transtensional folding Haakon Fossen a, *, Christian Teyssier b, Donna L. Whitney b a Department of Earth Science, Museum of Natural History, University of Bergen, Postboks 7803, N-5007 Bergen, Norway b Department of Earth Sciences, University of Minnesota, Minneapolis, MN 55455, USA article info abstract Article history: Strain modeling shows that folds can form in transtension, particularly in simple shear-dominated Received 19 July 2013 transtension. Folds that develop in transtension do not rotate toward the shear zone boundary, as Received in revised form they do in transpression; instead they rotate toward the divergence vector, a useful feature for deter- 3 September 2013 mining past relative plate motions. Transtension folds can only accumulate a fixed amount of horizontal Accepted 11 September 2013 shortening and tightness that are prescribed by the angle of oblique divergence, regardless of finite Available online 20 September 2013 strain. Hinge-parallel stretching of transtensional folds always exceeds hinge-perpendicular shortening, causing constrictional fabrics and hinge-parallel boudinage to develop. Keywords: Transtension These theoretical results are applied to structures that developed during oblique continental rifting in Folding the upper crust (seismic/brittle) and the ductile crust. Examples include (1) oblique opening of the Gulf Shear zones of California, where folds and normal faults developed simultaneously in syn-divergence basins; (2) Oblique divergence incipient continental break-up in the Eastern California-Walker Lane shear zone, where earthquake focal Constrictional strain mechanisms reflect bulk constrictional strain; and (3) exhumation of the ultrahigh-pressure terrain in SW Norway in which transtensional folds and large magnitude stretching developed in the footwall of detachment shear zones, consistent with constrictional strain. -
Artificial Groundwater Recharge – Is It Possible in Mozambique?
Artificial groundwater recharge – is it possible in Mozambique? Johanna Alexson Dissertations in Geology at Lund University, Bachelor’s thesis, no. 369 (15 hp/ECTS credits) Department of Geology Lund University 2013 Artificial groundwater recharge – is it possible in Mozambique? Bachelor’s thesis Johanna Alexson Department of Geology Lund University 2013 Contents 1 Introduction ......................................................................................................................................................... 5 2 Method ................................................................................................................................................................. 5 3 Artificial recharge systems and their purpose .................................................................................................. 5 3.1 Different purposes 5 3.2 Artificial recharge systems 5 4 Requirements ...................................................................................................................................................... 7 4.1 Experience 7 4.2 Sediment properties and problems 7 4.2.1 Soil 7 4.2.2 Clogging 8 4.3 Surface- and groundwater chemistry and availability 8 4.3.1 Water chemistry 8 4.3.2 Surface water chemistry 10 4.3.3 Groundwater chemistry 10 4.3.4 Availability 10 4.4 Water improvement options 10 4.4.1 Oxidation 10 4.4.2 Disinfection 10 4.4.3 Corrosion correction 11 5. Conditions of Mozambique ............................................................................................................................ -
Descriptive Text to the 1995 Geological Map of Greenland, 1:2 500 000
GEOLOGICAL SURVEY OF DENMARK AND GREENLAND BULLETIN 18 2009 Greenland from Archaean to Quaternary Descriptive text to the 1995 Geological map of Greenland, 1:2 500 000. 2nd edition Niels Henriksen, A.K. Higgins, Feiko Kalsbeek and T. Christopher R. Pulvertaft GEOLOGICAL SURVEY OF DENMARK AND GREENLAND MINISTRY OF CLIMATE AND ENERGY Geological Survey of Denmark and Greenland Bulletin 18 Keywords Archaean, Caledonides, Cenozoic, economic geology, geological map, Greenland, ice sheet, Mesozoic, offshore, orogenic belts, Palaeozoic, petroleum, Phanerozoic, Proterozoic, sedimentary basins. Cover illustration The cover design depicts mountains of the East Greenland Caledonian fold belt. The view, west of Mestersvig (located on map, page 4), is north over Bersærkerbræ and the northern part of the Stauning Alper to Kong Oscar Fjord with Traill Ø in the right backgro- und. The mountains up to 1800 m high are of the Neoproterozoic Eleonore Bay Supergroup. To the right: first author Niels Henriksen, for many years head of geological mapping at GGU/GEUS, and participant in field work in Greenland for more than 45 years. Frontispiece: facing page Major Caledonian syncline involving reactivated Archaean basement gneisses containing amphibolite bands. Overlying rusty coloured Mesoproterozoic metasediments (Krummedal supracrustal sequence) just visible in tight core of the fold. The intensity of deformation in the syncline clearly increases towards the core, where the basement gneisses become more strongly foliated. Some of the amphibolite bands were derived from cross-cutting basic intrusions, which are still discernable in the less severely deformed parts of the Archaean basement (Fig. 17, p. 31). The height of the section is c. 2000 m.